(Table 1) Organic carbon, nitrogen and sulphur concentrations and δ¹³C of TOC from ODP Hole 167-1017E sediments

DOI

A high-resolution analysis of Hole 1017E revealed that total organic carbon (TOC) concentrations (24.8 ± 2.9 mg/g) and d13C of TOC (-21.3 ± 0.2 per mil) in Holocene sections are higher than those in glacial sediments (14.2 ± 4.8 mg/g and -22.1 per mil ± 0.1 per mil, respectively). The 306- to 280-cm section has high total sulfur concentrations, which may correspond to anoxia Event 1 (1 of the warm interstadials of GISP2) in the Santa Barbara Basin.

Supplement to: Ishiwatari, Ryoshi; Matsumoto, Kohei; Seki, Osamu; Yamamoto, Shuichi (2000): Variations in organic carbon isotopic composition in sediments at Site 1017 during the last 25 k.y. In: Lyle, M; Koizumi, I; Richter, C; Moore, TC Jr (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 167, 1-4

Identifier
DOI https://doi.org/10.1594/PANGAEA.796267
Related Identifier https://doi.org/10.2973/odp.proc.sr.167.210.2000
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.796267
Provenance
Creator Ishiwatari, Ryoshi; Matsumoto, Kohei; Seki, Osamu; Yamamoto, Shuichi
Publisher PANGAEA
Publication Year 2000
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 1377 data points
Discipline Earth System Research
Spatial Coverage (-121.107 LON, 34.535 LAT); North Pacific Ocean
Temporal Coverage Begin 1996-05-28T02:00:00Z
Temporal Coverage End 1996-05-28T06:30:00Z